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《EARTH SCIENCE FRONTIERS》 1995-01
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AN OVERVIEW OF METAMORPHIC CORE COMPLEXES───CHARACTERISTICS AND ORIGIN

Song Honglin(China University of Geosciences,Beijing,100083)  
Comparing the characteristics of metamorphic core complexes(MCC)of Chinaand abroad,several points have been emphasized:(1)The tectonic setting of MCC,thereare two kinds of MCC,located on the margin of cratons,such as Cordilleran MCC,orwithin cratons,such as most MCC found in the North China craton. (2)The MCC arecharacterized by three-layer configuration, instead of two-plate mode suggested for thecordilleran MCC,In addition to the metamorphic core and unmetamorphic cover plate,there is an intermediate ductile slab characterized by non-coaxial ductile flow of low-grademeta-sedimentary sequnces,especially in the older MCC, such as Mesozoic MCC in Chi-na.(3)Horizontal heterogeneous distribution of intermediate ductile flow slab indicatesthe lateral inhomogeneity of the thermal state in the crust.(4) From the geometry,dy-namics,thermal state,magmatism and metamorphism of MCC,it is suggested that a com-bination of heating from mantle,thermal-induced softening of the crust,buoying of theheating core and horizontal shear stress may be the cause of the uplift of MCC.
【Fund】: 地质矿产部重大基础地质项目
【CateGory Index】: P588.3
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